001     52930
005     20240712100912.0
017 _ _ |a An edited version of this paper was published by AGU. Copyright 2001 American Geophysical Union. To view the published open abstract, go to http://dx.doi.org/10.1029/2006GL026925
024 7 _ |a 10.1029/2006GL026925
|2 DOI
024 7 _ |a WOS:000241699700001
|2 WOS
024 7 _ |a 2128/580
|2 Handle
037 _ _ |a PreJuSER-52930
041 _ _ |a eng
082 _ _ |a 550
084 _ _ |2 WoS
|a Geosciences, Multidisciplinary
100 1 _ |a Tilmes, S.
|0 P:(DE-Juel1)VDB1652
|b 0
|u FZJ
245 _ _ |a Chemical ozone loss in the Arctic and Antarctic stratosphere between 1992 and 2005
260 _ _ |a Washington, DC
|b American Geophysical Union
|c 2006
300 _ _ |a L20812
336 7 _ |a Journal Article
|0 PUB:(DE-HGF)16
|2 PUB:(DE-HGF)
336 7 _ |a Output Types/Journal article
|2 DataCite
336 7 _ |a Journal Article
|0 0
|2 EndNote
336 7 _ |a ARTICLE
|2 BibTeX
336 7 _ |a JOURNAL_ARTICLE
|2 ORCID
336 7 _ |a article
|2 DRIVER
440 _ 0 |a Geophysical Research Letters
|x 0094-8276
|0 2249
|v 33
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a [1] The magnitude of chemical loss of polar ozone induced by anthropogenic halogens depends on the extent of chlorine activation, which is controlled by polar stratospheric clouds (PSCs) and thus by temperature. We propose a new quantity, the PSC formation potential (PFP) of the polar vortex, suitable for comparing the amount of ozone depletion in the Arctic and Antarctic regions. PFP represents the fraction of the vortex, over an ozone loss season, exposed to PSC temperatures. Chemical ozone loss in the Arctic correlates well with PFP, for winters between 1991 and 2005. For Antarctic and cold Arctic winters, PFP has been increasing over the past 30 years. In winter 2005, PFP and ozone loss in the Arctic reached record highs, approaching Antarctic levels. Nevertheless, column ozone in spring in the Arctic is much larger than the Antarctic, because of larger dynamical resupply of ozone to the Arctic.
536 _ _ |a Atmosphäre und Klima
|c P22
|2 G:(DE-HGF)
|0 G:(DE-Juel1)FUEK406
|x 0
588 _ _ |a Dataset connected to Web of Science
650 _ 7 |a J
|2 WoSType
700 1 _ |a Müller, R.
|0 P:(DE-Juel1)129138
|b 1
|u FZJ
700 1 _ |a Engel, A.
|0 P:(DE-Juel1)VDB352
|b 2
|u FZJ
700 1 _ |a Rex, M.
|0 P:(DE-Juel1)VDB8772
|b 3
|u FZJ
700 1 _ |a Russell, J. M.
|0 P:(DE-HGF)0
|b 4
773 _ _ |a 10.1029/2006GL026925
|g Vol. 33, p. L20812
|p L20812
|q 33|0 PERI:(DE-600)2021599-X
|t Geophysical research letters
|v 33
|y 2006
|x 0094-8276
856 7 _ |u http://dx.doi.org/10.1029/2006GL026925
|u http://hdl.handle.net/2128/580
856 4 _ |u https://juser.fz-juelich.de/record/52930/files/bipol_grls.pdf
|y OpenAccess
856 4 _ |u https://juser.fz-juelich.de/record/52930/files/bipol_grls.jpg?subformat=icon-1440
|x icon-1440
|y OpenAccess
856 4 _ |u https://juser.fz-juelich.de/record/52930/files/bipol_grls.jpg?subformat=icon-180
|x icon-180
|y OpenAccess
856 4 _ |u https://juser.fz-juelich.de/record/52930/files/bipol_grls.jpg?subformat=icon-640
|x icon-640
|y OpenAccess
909 C O |o oai:juser.fz-juelich.de:52930
|p openaire
|p open_access
|p driver
|p VDB
|p dnbdelivery
913 1 _ |k P22
|v Atmosphäre und Klima
|l Atmosphäre und Klima
|b Umwelt
|z fortgesetzt als P23
|0 G:(DE-Juel1)FUEK406
|x 0
914 1 _ |y 2006
915 _ _ |0 StatID:(DE-HGF)0010
|a JCR/ISI refereed
915 _ _ |2 StatID
|0 StatID:(DE-HGF)0510
|a OpenAccess
920 1 _ |k ICG-I
|l Stratosphäre
|d 31.12.2006
|g ICG
|0 I:(DE-Juel1)VDB47
|x 0
970 _ _ |a VDB:(DE-Juel1)83264
980 1 _ |a FullTexts
980 _ _ |a VDB
980 _ _ |a JUWEL
980 _ _ |a ConvertedRecord
980 _ _ |a journal
980 _ _ |a I:(DE-Juel1)IEK-7-20101013
980 _ _ |a UNRESTRICTED
980 _ _ |a FullTexts
981 _ _ |a I:(DE-Juel1)ICE-4-20101013
981 _ _ |a I:(DE-Juel1)IEK-7-20101013


LibraryCollectionCLSMajorCLSMinorLanguageAuthor
Marc 21